Mesoarchean
Aeonothem | Arathem | system | Age ( mya ) |
---|---|---|---|
later | later | later | |
A r c h a i k u m Duration: 1500 Ma |
Neo-Archaic Duration: 300 Ma |
2500 ⬍ 2800 |
|
Mesoarchean Duration: 400 Ma |
2800 ⬍ 3200 |
||
Paleoarchean Duration: 400 Ma |
3200 ⬍ 3600 |
||
Eoarchic Duration: 400 Ma |
3600 ⬍ 4000 |
||
formerly: Hadaikum |
The Mesoarchean is a geological era . It represents the third of four eras within the geological eon of the Archean (Mesoarchean = "middle Archean"). It begins about 3200 million years ago BP with the end of the Paleoarchean and ends about 2800 million years ago BP with the beginning of the Neoarchean . Its duration is 400 million years.
Redefinition of the Mesoarchean
In the course of moving away from period boundaries determined purely by radiometry, the GSSP principle should now be applied as far as possible in the Precambrian, according to Gradstein et al. (2012) . Periods are now defined in terms of significant geological events rather than arbitrary radiometric ages.
Since the Eoarchaic no longer applies, according to Gradstein, the Mesoarchaic begins much earlier, namely at the GSSP of the Vaalbarum , which is set at 3490 million years BP. This GSSP comes to lie at the lower edge of the Dresser Formation belonging to the West Australian Warrawoona Group , which concordantly overlays the pillow basalts of the North Star Basalt . The Vaalbarum follows as the second period of the Mesoarchean at 3020 million years BP, the Pongolum , which is also defined by a GSSP (concordant contact between the basal conglomerate and the quartz-rich sandstone above it of the Gorge Creek Group ( De Gray Supergroup ) in Western Australia) . The Pongolum lasts until 2780 million years BP and is separated by a GSSP from the subsequent Neo-Archean or its first period, the Methanium . The GSSP, which concludes the Mesoarchean, is being relocated to the base of Mount Roe Basalt in Western Australia. The Mount Roe Basalt belongs to the Fortescue Group and thus to the Mount Bruce Supergroup . The newly defined Mesoarchean lasts a total of 710 million years.
meaning
The main characteristic of the Mesoarchean is undoubtedly the first appearance of macroscopically recognizable life . The oldest known stromatolites appear at the base of the Dresser Formation . After the meteorite bombardment has finally subsided, their spread is linked to the emergence of the first stable continents (or continent germs) and their floating lithospheric roots. The stromatolites in the Mkhonjwa Mountains northeast of Barberton in South Africa and in Steep Rock Lake, NW Ontario in Canada, in which fossils of cyanobacteria were found, date back to 3200 and 2800 million years ago BP.
With the Pongolum, terrestrial sedimentary basins appear for the first time , which were able to form on stabilized continents . In powerful, undisturbed sequences on shelf platforms , the colonization of flat, sandy areas of the facies by microbes can be demonstrated.
Icing
The Pongola glaciation occurred about 2,900 million years ago. It can be verified by two diamictite horizons in the Mozaan Group of the Pongola Supergroup ( Delfkom formation ).
Meteorite impacts
In the period 3470 to 3240 million years BP, four horizons were deposited within the Swaziland Supergroup of the South African Kaapvaal Kraton , which indicate possible meteorite impacts . The lowest horizon can also be found in the Warrawoona Group of the West Australian Pilbara Kraton .
stratigraphy
Significant geological formations
-
Pilbara Kraton in Western Australia :
-
Pilbara Supergroup in the East Pilbara Terrane - 3525 to 3230 million years BP
- Warrawoona Group - 3525 to 3426 million years BP
- Kelly Group - 3350 to 3315 million years old BP
- Sulfur Springs Group - 3255 to 3230 million years BP
- Roeburne Group in the western section - 3270 to 3250 million years BP
- Whundo Group at its center - 3125 to 3115 million years BP
-
De Gray Superbasin with the De Gray Supergroup :
- Gorge Creek Group - 3050 to 3020 million years old BP
- Whim Creek Group - 3010 to 2990 million years old BP
- Mallina Basin - 2970 to 2940 million years old BP
- Croydon Group - 2970 to 2940 million years BP
- Nullagine Group - 2930 to 2910 million years old BP
-
Pilbara Supergroup in the East Pilbara Terrane - 3525 to 3230 million years BP
-
North China Kraton - 3100 to 2900 million years BP:
- Quishui Group in eastern Shandong
- Longgang Group in southern Jilin
- Lower Anshan Group in northern Liaoning
- Qianan Supracrustals in eastern Hebei
- Chentaigou Supracrustals in Anshan
-
Dharwar Kraton in southern India :
- Sargur Group - 3100 to 2900 million years old BP
-
Dharwar supergroup
-
Bababundan Group - 2900 to 2600 million years BP
- Kalasapura Formation - around 2910 million years ago BP
- Santaveri Formation and Allampur Formation - 2848 to 2747 million years BP
-
Bababundan Group - 2900 to 2600 million years BP
-
Singhbhum Kraton in Northeast India:
- Iron Ore Group - 3100 to 2900 million years BP
-
Kaapvaal Kraton in South Africa :
-
Swaziland Supergroup - 3547 to 3100 million years BP
- Onverwacht Group - 3547 to 3260 million years BP
- Fig Tree Group - 3259 to 3225 million years BP
- Moodies Group - 3227 to 3110 million years old BP
- Dominion Group - 3090 to 3070 million years old BP
- Pongola Supergroup in South Africa and Swaziland - 3000 to 2870 million years BP
- Nsuze Group - 2980 to 2960 million years BP
- Mozaan Group - around 2950 to 2837 (?) Million years BP
-
Witwatersrand Supergroup in South Africa - 2985 to 2780 million years BP
- West Rand Group - 2985 to 2914 million years old BP
- Central Rand Group - 2872 to 2780 million years BP
-
Swaziland Supergroup - 3547 to 3100 million years BP
-
Antarctica :
- Nimrod Group in the Transantarctic Mountains - 3290 to 3060 million years BP. The very heterogeneous group was recorded by the Nimrod orogeny around 1730/1720 million years BP and by the Ross orogeny around 540/520 million years BP .
Deposits
-
Gold :
- Jamestown ophiolite of the Barberton greenstone belt , Kaapvaal Kraton (Main Reef Complex, Agnes Mine and Sheba Mine) - <3500 million years BP
- Red Lake greenstone belt of the Superior Craton with the Campbell-Red Lake orogenic gold deposit - 2990 to 2890 million years BP
- Gold and uranium :
- The Witwatersrand Supergroup (2985 to 2780 million years BP) in South Africa is home to the largest gold deposits in the world.
-
Nickel group :
- Barberton Greenstone Belt Jamestown Ophiolite, Kaapvaal Kraton (Bon Accord Nickel Deposit)
-
Chromium ( Chromite ):
- Nuggihalli Schist Belt , Sargur Group, South India
Magmatism
-
Greenstone belt :
- Jamestown ophiolite in the Barberton greenstone belt , Kaapvaal craton - around 3500 million years BP
- Sayan greenstone belt in the Sayan fold belt , Siberia Kraton - around 3200 million years BP
- Olondo greenstone belt in the Aldan shield , Siberia craton - 3065 to 2986 million years BP
Geodynamics
Orogenesis
-
Baltic shield :
- Saamium - 3100 to 2900 million years BP
- North Pilbara Orogeny - 2950 to 2910 million years BP. The Kurrana Terran is secreted in the southeast of the East Pilbara Block. The outcrop of postectonic granites between 2890 and 2830 million years BP leads to final cratonization.
See also: Geological timescale
Individual evidence
- ↑ Geology as a place of learning. ( Memento of the original from July 14, 2010 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. (PDF; 4.4 MB, p. 2) on the website of the Bavarian State Ministry for Environment and Health , www.stmug.bayern.de
- ↑ Thomas R. Becker: The measurement of earth time - a historical-methodological overview in: Ewige Moments: An interdisciplinary approach to the phenomenon of time. Ed .: Veronika Jüttemann, Waxmann Verlag, ISBN 978-3-8309-2011-3 , p. 57 books.google.de
- ^ Felix M. Gradstein et al .: On the Geologic Time Scale . In: Newsletters on Stratigraphy . tape 45/2 , 2012, p. 171-188 .
- ^ Stromatolites in the early days of the earth's history. ( Memento from July 31, 2012 in the web archive archive.today ) In: Faculty of Geosciences and Geography at the University of Göttingen
- ↑ Robert E. Kopp, Joseph L. Kirschvink, Isaac A. Hilburn, Cody Z. Nash: The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis . In: Proceedings of the National Academy of Sciences . tape 102 , no. 32 , August 9, 2005, ISSN 0027-8424 , p. 11131–11136 , doi : 10.1073 / pnas.0504878102 , PMC 1183582 (free full text).
- ↑ Roland Walter: Earth history: the formation of the continents and oceans. de Gruyter, Berlin 2003, ISBN 978-3-11-017697-1 , p. 51 books.google.de
- ↑ Lowe, DR et al .: Spherule beds 3.47 - 3.24 billion years old in the Barberton Greenstone Belt, South Africa: A record of large meteorite impacts and their influence on early crustal and biological evolution . In: Astrobiology . v. 3, 2003, p. 7-47 .
- ^ DR Lowe, GR Byerly: Stratigraphy of the west-central part of the Barberton Greenstone Belt, South Africa . In: DR Lowe, GR Byerly (Ed.): Geologic evolution of the Barberton Greenstone Belt, South Africa. Geological Society of America Special Paper . tape 329 , 1999, pp. 1-36 .
- ^ Axel Hofmann: The geochemistry of sedimentary rocks from the Fig Tree Group, Barberton greenstone belt. Implications for tectonic, hydrothermal and surface processes during mid-Archaean times . In: Precambrian Research . tape 143 , no. 1-4 , December 15, 2005, pp. 23-49 , doi : 10.1016 / j.precamres.2005.09.005 .
- ^ SL Kamo, SW Davis: Reassessment of Archean crustal development in the Barberton Mountain Land, South Africa, based on U-Pb dating . In: Tectonics . tape 13 , 1994, pp. 167-192 .
- ^ JW Goodge, CM Fanning: 2.5 billion years of punctuated Earth history as recorded in a single rock . In: Geology . tape 27 , 1999, p. 1007-1010 .
- ↑ JW Goodge, among others: U-PB evidence of 1.7 Ga crustal tectonism during the Nimrod Orogeny in the Transantarctic Mountains, Antarctica: implications for Proterozoic plate reconstructions . In: Precambrian Research . tape 112 , 2001, p. 261-288 .
- ^ MJ Robertson, among others: Gold mineralization during progressive deformation at the Main Reef Complex, Sheba Gold Mine, Barberton Greenstone Belt, South Africa . In: Africa. Econ. Geol. Res. Unit Inf. Circ. tape 267 . University of Witwatersrand, 1993, p. 1-26 .
- ^ G. Chi, inter alia: Formation of the Campbell-red Lake gold deposit by H 2 O-poor, CO 2 -dominated fluids . In: Mineralium deposita . tape 40 , 2006, pp. 726-741 .
- ^ SA De Waal: Nickel minerals from Barberton, South Africa. VII. The spinels Co-chromite and Ni-chromite and their significance for the origin of the Bon Accord nickel deposit . In: Bull.BRGM II (2), 1978, p. 223-230 .